Viscously damped acoustic waves with the
lattice Boltzmann method
By Erlend Magnus Viggen
Acoustics Group,Dept.of Electronics and Telecomm.,Norwegian University of
Science and Technology,O.S.Bragstads Plass 2,7034 Trondheim,Norway
Acoustic wave propagation in lattice Boltzmann BGK simulations may be analysed
using a linearization method.This method has been used in the past to study prop
agation of waves which are viscously damped in time,and is here extended to also
study waves which are viscously damped in space.Its validity is veriﬁed against
simulations,and the results are compared with theoretical expressions.It is found
in the inﬁnite resolution limit k →0 that the absorption coeﬃcients and phase dif
ferences between density and velocity waves match theoretical expressions for small
values of ωτ
ν
,the characteristic number for viscous acoustic damping.However,the
phase velocities and amplitude ratios between the waves increase incorrectly with
(ωτ
ν
)
2
,and agree with theory only in the inviscid limit k →0,ωτ
ν
→0.The actual
behaviour of simulated plane waves in the inﬁnite resolution limit is quantiﬁed.
Keywords:Lattice Boltzmann,wave propagation,computational aeroacoustics
1.Introduction
In a seminal article,Lighthill showed how ﬂow ﬁelds may act as acoustic sources [1],
thereby planting the seed for the scientiﬁc ﬁeld now known as aeroacoustics.The
related ﬁeld of computational aeroacoustics (CAA) has been studied since the 1980s,
and two main approaches of CAA have been identiﬁed:
The hybrid approach,where the ﬂow and acoustic ﬁelds are found separately.
The ﬂow ﬁeld is analysed to ﬁnd the acoustic source strength of the ﬂow,
which is then used to compute the acoustic ﬁeld in the surrounding domain.
The direct approach,where the acoustic ﬁeld comes out as a natural part of a
numerical solution to the compressible NavierStokes equation.
One important weakness of the hybrid approach is its inability to simulate the
feedback of the acoustic ﬁeld on the ﬂow ﬁeld.This means that it is not usable in
cases where this feedback is critical to the process of sound generation,such as in
the singing risers problem currently studied in the natural gas industry [2].It is
also diﬃcult to capture complex geometries with this method.
The direct approach has no such problems,but traditional numerical simulations
of the compressible NavierStokes equation are far more complex and demanding
than hybrid methods.It is therefore our hope that the lattice Boltzmann method
(LBM) can be used for direct CAA.Compared to traditional methods,the LBM is
straightforward to implement.It is also an explicit method which can be parallel
lized with a nearly linear speedup in number of processors.
Article submitted to Royal Society T
E
X Paper
2 E.M.Viggen
There exists a large body of work which validates the LBM as a useful tool for
simulations of incompressible ﬂow [3].However,it has been shown mathematically
that the LBM may also be used for solving the compressible NavierStokes equa
tion [4],albeit with spurious O(Ma
3
) terms which limit its applicability to small
Mach numbers and cause incomplete Galilean invariance.
To ascertain whether the LBM may become a useful tool for CAA,we need a
better picture of the acoustic behaviour of the method.This article will focus on
viscous damping of acoustic waves.In §2,the theory of this behaviour is described.
§3 describes a method of linearization analysis which can be applied to study this
behaviour in the LBM.The method is validated in §4,and is then used to compare
the behaviour of LBsimulated waves with theoretically expected behaviour.
2.Theoretical background
When performing the ChapmanEnskog analysis on the LBM,certain assumptions
must be made to retrieve the compressible NavierStokes equation.First,one as
sumes that the Mach number is suﬃciently low that the aforementioned spurious
terms can be neglected.Second,one assumes isothermal compression,so that the
absolute pressure and density p and ρ are linked through the thermodynamic speed
of sound c
s
= 1/
√
3 as p = c
2
s
ρ.These assumptions ﬁt well with those made in linear
acoustics:Low Mach number and adiabatic compression,so that the oﬀequilibrium
pressure and density p
′
and ρ
′
are linked as p
′
= c
2
s
ρ
′
.
One result of the ChapmanEnskog analysis is that the kinematic shear and bulk
viscosities for the BGK collision operator are given through the relaxation time τ
as respectively
ν = c
2
s
(τ −1/2),(2.1a)
ν
′
= 2ν/3.(2.1b)
This constant ratio between bulk and shear viscosities make it impossible to perform
simulations of ﬂuids with correct transport coeﬃcients without resorting either to
extended LB methods (e.g.[4]),or to another type of collision operator such as
the Multiple Relaxation Time (MRT) operator (e.g.[5]).Both these choices would
allow us to set bulk and shear viscosity independently.
(a) Solutions to the lossy wave equation
Conservation of mass and momentum are expressed through the continuity and
compressible NavierStokes equations,which relate density ρ,pressure p,and par
ticle velocity u,
∂ρ
∂t
= −∇ (ρu),(2.2a)
ρ
Du
Dt
= −∇p +ρ
4
3
ν +ν
′
∇(∇ u) −ρν∇×∇×u.(2.2b)
Assuming low Mach number,adiabatic compression,and suﬃcient distance to
boundaries,it may be shown similarly to ref.[6] that this implies a lossy wave
Article submitted to Royal Society
Damped acoustic waves with the LBM 3
equation,
1 +τ
ν
∂
∂t
∇
2
p −
1
c
2
s
∂
2
p
∂t
2
= 0,(2.3)
where τ
ν
= (
4
3
ν +ν
′
)/c
2
s
is the viscous relaxation time.Inserting from eq.2.1,we
ﬁnd for the LBM that τ
ν
= 2τ − 1.From the extended analysis of Hamilton &
Morfey [7],we see that eq.2.3 is correct up to second order in Mach number and
ωτ
ν
if the eﬀects of thermal conduction and molecular relaxation are neglected.
In one dimension,this equation implies general damped wave solutions in pres
sure,density,and particle velocity,
ˆp(x,t) = p
0
+ ˆp
′
e
i(ˆωt−
ˆ
kx)
,(2.4a)
ˆρ(x,t) = ρ
0
+ ˆρ
′
e
i(ˆωt−
ˆ
kx)
,(2.4b)
ˆu(x,t) = ˆu
′
e
i(ˆωt−
ˆ
kx)
,(2.4c)
where a hat implies a complex quantity,and ˆω = ω
′
+ iα
t
and
ˆ
k = k
′
− iα
x
are
complex angular frequency and complex wavenumber respectively.α
t
and α
x
are
the temporal and spatial absorption coeﬃcients,while the real parts ω
′
and k
′
are
linked through a phase velocity,c
p
= ω
′
/k
′
.By comparison,we have in lossless
media that
ˆ
k = k,ˆω = ω,and c
p
= ω/k = c
s
.
Two important special cases are temporal damping (when
ˆ
k = k) and spatial
damping (when ˆω = ω).In both cases,properties of the waves can be found by
inserting eq.2.4a into eq.2.3.For spatially damped waves,we thus ﬁnd
α
x
k
=
s
p
1 +(ωτ
ν
)
2
−1
2 +2(ωτ
ν
)
2
,
k
′
k
=
s
p
1 +(ωτ
ν
)
2
+1
2 +2(ωτ
ν
)
2
,
c
p
c
s
=
s
2 +2(ωτ
ν
)
2
p
1 +(ωτ
ν
)
2
+1
,
(2.5)
whereas for temporally damped waves we ﬁnd
α
t
/ω = ωτ
ν
/2,ω
′
/ω =
p
1 −(ωτ
ν
)
2
/4,c
p
/c
s
=
p
1 −(ωτ
ν
)
2
/4.(2.6)
These expressions only depend on the dimensionless quantity ωτ
ν
,which may be
seen as a characteristic dimensionless number for the eﬀect of viscous acoustic
damping.Spatially damped waves occur whenever a wave is radiated froman acous
tic source in an absorbing medium,and is the type commonly encountered in nature.
Early numerical studies of wave propagation with the LBM focused on tempo
rally damped waves,propagating a single wavelength in a periodic system[8].Later
numerical studies have taken spatial damping into account as well [9].
(b) Linearization of conservation equations
By inserting the damped wave solutions in eq.2.4 into the conservation equa
tions in eq.2.2 under the linearizing assumptions that the wave amplitudes ˆp
′
,ˆρ
′
,
and ˆu
′
are very small,we may reduce these equations to relations between the
complex wave amplitudes,
ˆu
′
/ˆρ
′
= ˆω/ρ
0
ˆ
k,(2.7a)
ˆp
′
/ˆu
′
= ρ
0
ˆω/
ˆ
k −iρ
0
ˆ
k (4ν/3 +ν
′
).(2.7b)
Article submitted to Royal Society
4 E.M.Viggen
The absolute values of these ratios indicate the amplitude ratios between the waves,
while the complex phases describe the phase diﬀerence between them.For temporal
and spatial damping,we may use expressions from eqs.2.5 and 2.6.
3.Linearization analysis of lattice Boltzmann
The acoustic behaviour of LB may be analysed by performing a similar lineariza
tion [4,5].We assume that we have a rest state F
eq
i
of density ρ
0
with a ﬂuctuation
ˆ
f
i
on top.We assume this to be on a general complex onedimensional wave form,
ˆ
f
i
(x,t) =
ˆ
h
i
e
i(ˆωt−
ˆ
kx)
.(3.1)
If this wave is very small,we may linearize the equilibrium distribution,
ˆ
f
eq
i
+F
eq
i
= ˆρt
i
1 +3ˆuc
i
+9(ˆuc
i
)
2
/2 −3ˆu
2
/2
,
ˆ
f
eq
i
≃ t
i
[(ˆρ −ρ
0
) +3ρ
0
ˆuc
i
].
(3.2)
In this smallamplitude limit,the aforementioned O(Ma
3
) errors disappear.
While this behaviour could be examined for a number of diﬀerent lattices,we will
follow ref.[10] and limit ourselves to the D1Q3 lattice,which is a onedimensional
projection of a number of common lattices (D2Q9,D3Q15,D3Q19,and D3Q27).
Thus,plane waves in D1Q3 are equivalent with plane waves along any main axis of
these other lattices.The D1Q3 lattice is given by velocities [c
−
,c
0
,c
+
] = [−1,0,1]
and weights [t
−
,t
0
,t
+
] = [1/6,2/3,1/6].
With density and momentum given as
ˆρ(x,t) = ρ
0
+
X
i
ˆ
f
i
(x,t) = ρ
0
+(
ˆ
h
−
+
ˆ
h
0
+
ˆ
h
+
)e
i(ˆωt−
ˆ
kx)
,(3.3a)
ρ
0
ˆu(x,t) =
X
i
c
i
ˆ
f
i
(x,t) = (
ˆ
h
+
−
ˆ
h
−
)e
i(ˆωt−
ˆ
kx)
,(3.3b)
we ﬁnd a postcollision distribution
ˆg
i
(x,t) =
ˆ
f
i
(x +c
i
,t +1) =
1 −
1
τ
ˆ
f
i
(x,t) +
1
τ
ˆ
f
eq
i
(x,t)
=
1 −
1
τ
ˆ
h
i
+
t
i
τ
h
ˆ
h
−
+
ˆ
h
0
+
ˆ
h
+
+3c
i
(
ˆ
h
+
−
ˆ
h
−
)
i
e
i(ˆωt−
ˆ
kx)
.
(3.4)
If we for simplicity assume x and t such that e
i(ˆωt−
ˆ
kx)
= 1,we ﬁnd
ˆ
f
i
(x,t +1) = ˆg
i
(x −c
i
,t) ⇒
ˆ
h
i
e
iˆω
= ˆg
i
(x,t)e
i
ˆ
kc
i
,(3.5)
which results in the eigenvalue problem as found in ref.[4],
1
3
e
−i
ˆ
k
(3 −1/τ) e
−i
ˆ
k
/2τ −e
−i
ˆ
k
/τ
2/τ 3 −1/τ 2/τ
−e
i
ˆ
k
/τ e
i
ˆ
k
/2τ e
i
ˆ
k
(3 −1/τ)
ˆ
h
−
ˆ
h
0
ˆ
h
+
= e
iˆω
ˆ
h
−
ˆ
h
0
ˆ
h
+
.(3.6)
Article submitted to Royal Society
Damped acoustic waves with the LBM 5
Through assuming
ˆ
k = k known and ﬁnding the eigenvalue e
iˆω
numerically,we
may study the behaviour of temporally damped waves in the LBM.Alternatively,
we may assume ˆω = ω known and ﬁnd the value of
ˆ
k which gives the correct
eigenvalue e
iω
through a nested binary search in k
′
and α
x
.This allows us to study
the behaviour of spatially damped waves also.
The eigenvector itself may be used to determine the relative complex amplitudes
ˆρ
′
and ρ
0
ˆu
′
of the density and velocity waves.It may be found from eqs.2.4 and
3.3 that ˆρ
′
=
ˆ
h
−
+
ˆ
h
0
+
ˆ
h
+
and ρ
0
ˆu
′
=
ˆ
h
+
−
ˆ
h
−
,so that
ρ
0
ˆu
′
ˆρ
′
=
ˆ
h
+
−
ˆ
h
−
ˆ
h
−
+
ˆ
h
0
+
ˆ
h
+
.(3.7)
In this way we may compare the ratios of the LB amplitudes with theoretical ones
from eq.2.7a.
4.Results
We may validate the linearization method by comparing with actual LBsimulations.
A spatially damped plane wave may be created in a simple fashion in a D1Q3 lattice
by pinning density and velocity to small sinusoidal functions around an equilibrium,
setting ρ(0,t) = ρ
0
+ ˆρ
′
 sin(ωt),u(0,t) = ˆu
′
 sin(ωt +∠[ˆu
′
/ˆρ
′
]) in the ﬁrst node
and always relaxing it to equilibrium.We may then measure the phase velocities
and absorption coeﬃcients of the resulting waves.
0 0.05 0.10 0.15
0.575
0.576
0.577
0.578
c
s
k
2
cp
Meas.spat.
Pred.spat.
Theor.spat.
Pred.temp.
Theor.temp.
(a) Phase velocity
0 0.05 0.10 0.15
1.57
1.58
1.59
1.6
∙10
−2
k
2
Meas.α
x
/k
Pred.α
x
/k
Theor.α
x
/k
Pred.α
t
/ω
Theor.α
t
/ω
(b) Normalized absorption coeﬃcients
Figure 1.Comparison of predicted LB and measured phase velocity and normalized ab
sorption coeﬃcients for spatially and temporally damped waves at ωτ
ν
= 2π ×5 ×10
−3
with theoretical values from eqs.2.5 and 2.6.
The comparison is performed in Figure 1,where we also compare with theoretical
values.We see that the linearization analysis for spatially damped waves accurately
predicts the values measured from simulations,validating this method as a tool
for predicting the behaviour of spatially damped waves.Validation for temporally
damped waves has already been performed [4].From this point,we will therefore
use the linearization analysis to study the behaviour of LB waves.
Article submitted to Royal Society
6 E.M.Viggen
The theoretical values in eqs.2.5 and 2.6 change only with the dimensionless
parameter ωτ
ν
.Our analysis shows that the LB phase velocity has a small numerical
dispersion which for low k is linear in k
2
.This k
2
error also aﬀects the spatial
absorption coeﬃcient,while the temporal absorption coeﬃcient is hardly inﬂuenced
in this way,being instead mainly aﬀected by a very small k
4
error.
In addition,the values for the phase velocity and absorption coeﬃcients do not
agree even when the numerical resolution goes to inﬁnity (the k →0 limit),which
means that the LBM with the BGK operator does not appear to be a consistent
method for simulating waves.We will now examine how the waves behave in this
limit.
0 0.005 0.01 0.015 0.02
0.576
0.578
0.580
0.582
0.584
c
s
(ωτ
ν
)
2
cp
Pred.spat.
Theor.spat.
Pred.temp.
Theor.temp.
(a) Phase velocity
0 0.001 0.002
−1.2
−0.8
−0.4
0
0.4
∙10
−3
(ωτ
ν
)
3
Pred.− theor.,α
x
/k.
Pred.− theor.,α
t
/ω.
(b) Normalized absorption coeﬃcient errors
Figure 2.Comparison of predicted LB and theoretical phase velocity and normalized
absorption coeﬃcients in k →0 limit as function of ωτ
ν
.
Figure 2 compares the behaviour of LB waves in this limit with theoretical
behaviour.We ﬁnd an agreement with theory and ChapmanEnskog analysis in the
k → 0,ωτ
ν
→ 0 limit for both phase velocity and absorption.The phase velocity
is a linear function of (ωτ
ν
)
2
as expected,but the slope is too steep in both cases.
The absorption is correct apart from some small errors in (ωτ
ν
)
3
.
Finally,we compare the ratio ρ
0
ˆu
′
/ˆρ
′
,as given from theory (eq.2.7a) and as
predicted through the linearization analysis (eq.3.7).From Figure 3,we see that
the amplitudes of the waves are linear functions of (ωτ
ν
)
2
,but that the slope of
spatially and temporally damped waves are again both steeper than they should
be.The phase shift is largely correct,with a small (ωτ
ν
)
3
error for spatially damped
waves and an insigniﬁcant (ωτ
ν
)
5
error for temporally damped waves.Again,the
results agree with theory in the k →0,ωτ
ν
→0 limit.
We have seen that the waves’ properties are quite wellbehaved,although not
necessarily correct.Table 1 compares the LB and theoretical properties of the waves
we have studied in the k → 0 limit,with terms of order O([ωτ
ν
]
3
) or higher ne
glected.We ﬁnd that the while the normalized absorption coeﬃcients and phase
shifts are consistent with theory in this limit,the phase velocities and amplitude
ratios do not match except in the inviscid limit.In fact,both of these increase at
rates which are (ωτ
ν
)
2
/4 greater than they should be.
Article submitted to Royal Society
Damped acoustic waves with the LBM 7
0 0.005 0.01 0.015 0.02
0.576
0.578
0.580
0.582
0.584
c
s
(ωτ
ν
)
2
ρ0
ˆu′
/ˆρ′

Pred.spat.
Theor.spat.
Pred.temp.
Theor.temp.
(a) Absolute value
0 0.001 0.002
−1.2
−0.8
−0.4
0
∙10
−3
(ωτ
ν
)
3
∠(ρ0
ˆu′
/ˆρ′)
Pred. theor.,spat.
Pred. theor.,temp.
(b) Complex phase angle error
Figure 3.Comparison of predicted LB and theoretical ratio between the complex wave
amplitudes ρ
0
ˆu
′
and ˆρ
′
.
Table 1.Wave properties in the k →0,small ωτ
ν
limit
(Tabulation of the predicted LB and theoretical properties of spatially and temporally
damped waves at inﬁnite resolution (k →0) when ωτ
ν
is small.α
∗
/∗ indicates normalized
absorption coeﬃcient for both types of damped waves.)
Type
c
p
/c
s
α
∗
/∗ ρ
0
ˆu
′
/ˆρ
′
/c
s
∠(ρ
0
ˆu
′
/ˆρ
′
)
Predicted spatial
1 +
5
8
(ωτ
ν
)
2
ωτ
ν
/2 1 +
1
2
(ωτ
ν
)
2
ωτ
ν
/2
Theoretical spatial
1 +
3
8
(ωτ
ν
)
2
ωτ
ν
/2 1 +
1
4
(ωτ
ν
)
2
ωτ
ν
/2
Predicted temporal
1 +
1
8
(ωτ
ν
)
2
ωτ
ν
/2 1 +
1
4
(ωτ
ν
)
2
ωτ
ν
/2
Theoretical temporal
1 −
1
8
(ωτ
ν
)
2
ωτ
ν
/2 1 ωτ
ν
/2
5.Conclusion
We have examined the behaviour of viscously damped LB waves using the BGK
collision operator.The linearization analysis was shown to be capable of analysing
not only temporally damped waves,but also spatially damped waves.
We found that while the absorption coeﬃcients and phase shifts match theory
well,the phase velocities and amplitude ratios do not,except in the limit of an
inviscid lossless ﬂuid.The results are valid for plane waves propagating along a
main axis in any lattice for which D1Q3 is a projection.The BGK operator allows
no freedom to aﬀect this,so addressing this problem would require an alternate
method.On the other hand,the actual behaviour in the inﬁnite resolution limit
k →0 has been quantiﬁed in Table 1,and the regularity of the deviations makes it
quite possible to predict LBphase velocities and absorption coeﬃcients a priori [11].
Since there is no independent pressure wave in the LBM,it is not possible to
perform comparisons with eq.2.7b.In fact,the ChapmanEnskog analysis for the
LBM assumes that p = c
2
s
ρ,which may be shown from eq.2.7 to be incorrect for
damped acoustic waves.That this incorrect assumption underlies the LBMmay be
a reason for the systematic deviations from theory which we have seen here.
Article submitted to Royal Society
8 E.M.Viggen
However,an extended energyconserving LBM has been proposed [12],and has
been validated for a number of compressible ﬂowproblems [13].Perhaps this method
would give results more consistent with theory.
The deviations are still quite small,and have been found to be comparable to
the ones found for highorder ﬁnite diﬀerence schemes [14].They also found the
LBM to be faster than highorder methods of similar accuracy.This indicates that
the LBM is a promising tool for CAA.
In this article,we have only looked at the eﬀects of viscosity on damped acoustic
waves.In real ﬂuids,there are very signiﬁcant contributions to this damping from
thermal conduction and molecular relaxation [6,15].It remains to be seen how the
LBM may be adapted to handle all three damping mechanisms.
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15 Blackstock,D.T.2000 Fundamentals of physical acoustics,ch.9,1st edn.John Wiley
& Sons
Article submitted to Royal Society
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